Ortogneises y metasedimentos de la formación infrabasal al Ollo de Sapo (Macizo de Hiendelaencina, Guadarrama Oriental)
This paper deals with an augengneis unit called Antonita-gneis. On the basis of their petrological and geochemical characteristies these gneisses are considered as oíd two-mica granites, with a silicosodic trend. These gneisses and their late manifestations (metaaplites and metapegmatites) are indud...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1981 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/6019 |
| Acesso em linha: | http://hdl.handle.net/10261/6019 |
| Access Level: | acceso abierto |
| Palavra-chave: | Formación Ollo de Sapo Sistema Central Ortogneises Metasedimentos |
| Resumo: | This paper deals with an augengneis unit called Antonita-gneis. On the basis of their petrological and geochemical characteristies these gneisses are considered as oíd two-mica granites, with a silicosodic trend. These gneisses and their late manifestations (metaaplites and metapegmatites) are induded in a metasedimentary series, belonging to the metamorphic grade of staurolite - kyanite. |
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